Computation of Geodesies on the Ellipsoid 142 [2] Brownlee, K. A., Statistical theory and methodology in science and engineering. New York, 1960. [3] Chernoff, H. and L. E. Moses, Elementary decision theory. New York, 1959. [4] Dantzig, D. van, Statistical priesthood (Savage on personal proba bilities). Statistica Neerlandica 11 (1957) page 1. [5] Luce, R. D. and H. Raiffa, Games and decisions. New York, 1954. [6] Monhemius, W., Besliskunde, een vlag die de lading dekt? Statistica Neerlandica 17 (1963) page 329. [7] Neumann, J. von, and O. Morgenstern, Theory of games and economie behaviour. Princeton, 1947. [8] Sadowski, W., The theory of decision-making. An introduction to operations research. Warszawa, 1965. [9] Savage, L. J., The foundations of statistics. New York, 1954. [10] Wald, A., Statistical decision functions. New York, 1950. Ir. J. C. P. DE KRUIF, Computing Centre of the Delft Geodetic Institute: 1. Principles of the method 1.1 Description of the problem. An arbitrary line on an ellipsoid can be described by four simul taneous differential equations, a geodesic by only three. These differential equations are of the elliptic type; they can only be solved by methods of the numerical analysis. One of these methods is a Taylor expansion (e.g. the formulas of Gauss and Legendre). This method however is not so suitable for use with a computer, because the number of derivatives of the differential equations, that must be taken into account, depends on the length of the line and the accuracy required. For a general formula-system this great number of derivatives causes a compli cated program. This method is well suited for computations concerning lines of about the same length in a fixed area. In that case the formulas can be simplified and the coefficients of the formulas can be tabulated somehow. The method to be described in this paper has been designed for computer use and is valid for lines of any length. 1.2 Principles of the solution. The system of simultaneous differential equations can be numeri cally solved by the method of Runge-Kutta. This method is directly based on the differential equations. The solution is valid for lines of any lengththe accuracy can be influenced by varying the step size.

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Tijdschrift voor Kadaster en Landmeetkunde (KenL) | 1967 | | pagina 7